Ec. Weatherhead et al., ANALYSIS OF LONG-TERM BEHAVIOR OF ULTRAVIOLET-RADIATION MEASURED BY ROBERTSON-BERGER METERS AT 14 SITES IN THE UNITED-STATES, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D7), 1997, pp. 8737-8754
Surface ultraviolet (UV) radiation measurements from the Robertson-Ber
l (RB) meter network and existing documentation of these data were exa
mined to determine long-term variations of UV. RB meter data from 14 s
ites in the United States were analyzed for trends over the period 197
4-1991. A more in-depth analysis of the RB meter data, including the u
se of supporting geophysical data, was carried out for four of the loc
ations. Results based on analysis of data from the 14 sites show a sig
nificant negative trend of the order of -6% per decade overall, reason
ably consistent with annual trends obtained by Scotto et al. [1988] us
ing similar data for the period 1974-1985. However, when allowance is
made for mean level shifts in the data for several of the stations aro
und 1979, which may be due to calibration anti other instrument-relate
d problems, the resulting overall trend is found to be of the order of
+2% per decade and not statistically significant. An additional trend
analysis using only RB meter data since 1979 at the 14 sites is also
performed and leads to overall trend results similar to those from til
e analysis which allows for mean level shifts in the data. The more de
tailed analysis of data from four of the stations for the period 1979-
1991 is performed to investigate the extent to which the trend behavio
r in the RB meter measurements call be explained by the behavior of ot
her geophysical quantities such as cloudiness and total ozone. In part
icular, radiative transfer model-based calculations of ultraviolet irr
adiance based on satellite data from the total ozone mapping spectrome
ter are compared with the RB meter measurements to help explain their
behavior. Generally, inconsistencies are found between the trend behav
ior in RB meter measurements and radiative transfer calculations, with
the RB data showing substantial downward movement relative to the cal
culations for three of the four sites. Significant evidence exists to
indicate that problems with the network render the existing RB meter m
easurements unreliable for long-term trend detection. Different reason
able treatments of the data result in dramatically different trend res
ults. Without further information, the data, by themselves, do not all
ow for definitive trend analysis results.